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<front>
<journal-meta>
<journal-id journal-id-type="archive">gsminmag</journal-id>
<journal-title>Mineralogical Magazine</journal-title>
<abbrev-journal-title abbrev-type="full">Mineralogical Magazine</abbrev-journal-title>
<issn pub-type="ppub">0026-461X</issn>
<publisher>
<publisher-name>Mineralogical Society</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1180/minmag.1960.032.248.07</article-id>
<title-group>
<article-title>Two Synthetic Compounds Containing Chromium in Different Valency States</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Johnson</surname>
<given-names>W.</given-names>
</name><degrees>M.A.</degrees>
<aff>The United Steel Companies Limited, Research and Development Dept., Swinden Laboratories, Moorgate, Rotherham, Yorkshire.</aff></contrib></contrib-group>
<pub-date pub-type="ppub">
<month>3</month>
<year>1960</year>
</pub-date>
<volume>32</volume>
<issue>248</issue>
<fpage>408</fpage>
<lpage>411</lpage>
<copyright-statement>Copyright &#x00A9; 1960, The Mineralogical Society</copyright-statement>
<copyright-year>1960</copyright-year>
<abstract>
<title>Summary</title>
<p>Two compounds, one an apatite and the other a perovskite, have been synthesized by sintering mixtures containing CaO and Cr<sub>2</sub>O<sub>3</sub>, and CaO, Cr<sub>2</sub>O<sub>3</sub>, and Fe<sub>2</sub>O<sub>3</sub> respectively. The apatite formed by partial oxidation of the Cr<sub>2</sub>O<sub>3</sub> and subsequent pick-up of moisture from the atmosphere, to give Ca<sub>5</sub>(CrO<sub>4</sub>)<sub>3</sub>OH. The perov-skite formed as a non-stoicheiometric compound Ca<sub>4</sub>(Fe,Cr)<sub>4</sub>O<sub>11</sub> by partial oxidation of the Cr<sub>2</sub>O<sub>3</sub> during firing. Lattice parameters and interplanar spacings are given for the two structures.</p></abstract>
</article-meta>
</front>
</article>
